Earth’s Crust Earth is covered by a rock layer called the crust.. Rocks slowly break into smaller pieces.. Physical WeatheringIn physical weathering, rock breaks into smaller pieces of t
Trang 1by Marcia K Miller
Scott Foresman Science 4.9
Genre Comprehension Skill Text Features Science Content
Nonfi ction Compare and
Contrast
• Labels
• Captions
• Diagrams
• Glossary
Earth’s Surface
ISBN 0-328-13883-5
ì<(sk$m)=bdiidi< +^-Ä-U-Ä-U
Earth Science
by Marcia K Miller
Scott Foresman Science 4.9
Genre Comprehension Skill Text Features Science Content
Nonfi ction Compare and
Contrast
• Labels
• Captions
• Diagrams
• Glossary
Earth’s Surface
ISBN 0-328-13883-5
ì<(sk$m)=bdiidi< +^-Ä-U-Ä-U
Earth Science
Trang 2deposition
earthquake
epicenter
erosion
fault
landform
landslide
volcano
weathering
What did you learn?
1 What can cause a landslide?
2 What makes magma rise inside a volcano?
3 Why do earthquakes happen at faults?
4 Erosion and deposition are two forces that change landforms Explain in your own words what each force does Include details from the book to support your answer.
weathering and chemical weathering alike? How are they different?
Illustration: 14 Alan Male
Photographs: Every effort has been made to secure permission and provide appropriate credit for
photographic material The publisher deeply regrets any omission and pledges to correct errors called to its
attention in subsequent editions Unless otherwise acknowledged, all photographs are the property of Scott
Foresman, a division of Pearson Education Photo locators denoted as follows: Top (T), Center (C), Bottom
(B), Left (L), Right (R) Background (Bkgd)
Opener: ©Hubert Stadler/Corbis; Title Page: ©Chris Reynolds and the BBC Team-Modlemakes/DK
Images; 4 ©AP/Wide World Photos; 5 ©Jack Dykinga/Getty Images; 7 (T) ©Richard Bickel/Corbis, (B)
©Owaki-Kulla/Corbis; 8 ©Paul A Souders/Corbis; 10 ©Dave G Houser/Corbis; 13 (TR, CR) ©Gary
Rosenquist; 15 ©George Hall/Corbis
ISBN: 0-328-13883-5
Copyright © Pearson Education, Inc
All Rights Reserved Printed in the United States of America This publication is
protected by Copyright and permission should be obtained from the publisher prior
to any prohibited reproduction, storage in a retrieval system, or transmission in any
form by any means, electronic, mechanical, photocopying, recording, or likewise For
information regarding permissions, write to: Permissions Department, Scott Foresman,
1900 East Lake Avenue, Glenview, Illinois 60025.
3 4 5 6 7 8 9 10 V010 13 12 11 10 09 08 07 06 05
Changes to Earth’s Surface
by Marcia K Miller
Trang 3How does Earth’s
surface wear away?
Earth’s Crust
Earth is covered by a rock layer called the crust The crust
is underwater in the ocean
Earth’s crust has many natural features Each one is called
a landform Landforms are many sizes and shapes Plains
are flat landforms on low ground Plateaus are flat landforms
on high ground Peninsulas are landforms that stick out into
water Valleys and canyons are also landforms
3
Some landforms develop quickly Others take a long time
A mountain may take millions of years to form Rocks rolling downward can change it quickly Think of how a flood moves soil from one place to another Think about dust that blows across empty, unplanted fields
How Weathering Affects Landforms
Landforms are always changing Rocks slowly break into
smaller pieces This process is called weathering Water, ice,
and temperature changes can cause weathering Chemicals and living things cause weathering too
Trang 4Physical Weathering
In physical weathering, rock breaks into smaller pieces of the same kind of rock Water can cause physical weathering Flowing water carries small bits
of soil and sand These bits scrape against rocks to wear them down
Ice also causes physical weathering Rain or melting snow can get into cracks in rocks If this water freezes, it turns into ice The ice pushes against the cracks The cracks become deeper This process can repeat until the rock finally splits
Changes in temperature can also weather rocks A rock’s surface grows larger when it gets hot Its surface shrinks when it gets cold All this changing may weaken the rock
Living things can also cause weathering Have you seen plants living in the cracks of rocks? As plants and roots grow, they can split the rocks
4
Weathering changed the rock known as the Old Man of the Mountain in New Hampshire In 2003 the rock broke off and fell.
Chemical Weathering
In chemical weathering, rock breaks into smaller pieces But the material that the rock is made of also changes
Different materials can be formed when chemicals come in contact with rock Carbon dioxide, a chemical in the air, mixes with rainwater and forms a weak acid When it rains, this acid lands on the rock It combines with rock material and forms
a new chemical Over time, the new chemical breaks the rock into smaller pieces
Chemicals can come from animals and plants These chemicals can cause weathering So can people and their activities
As water moves, it weathers rock and carries it to new places.
5
Trang 5How do weathered
materials move?
Effects of Erosion
Erosion is the process of moving weathered rock Water, ice,
gravity, and wind can cause erosion
Rain can wash away loose rock material into a stream The
stream may carry that material far away
Over time, water running downhill carves grooves into the
land These grooves become canyons or valleys
Waves pound against cracks in rocks that are at the shore
Pieces of rock break off and are carried away As the shore
erodes, new landforms, such as beaches, will appear
Millions of years ago, huge ice sheets, called glaciers, covered
parts of Earth A glacier slowly slides along a thin layer of water
below it, wearing away rock Even small glaciers can rip rocks
apart and carry the pieces far away
Deposition
Wind and water carry bits of rock and soil from one place
to another Deposition is the laying down of pieces of Earth’s
surface This may happen slowly or very quickly
When water moves slowly, big pebbles in the water sink first Then smaller bits, such as sand, sink Finally the smallest pieces
of soil, called silt, fall to the bottom Rivers deposit material where they meet the ocean This deposit forms a fan-shaped landform called a delta
Wind can carry only small bits of rock In deserts, the wind deposits sand in mounds called sand dunes Wind will keep shaping the dunes
Trang 6Gravity and Landslides
No place on Earth is completely flat The force of gravity
pulls all objects from high places to lower ones Gravity causes
loose material to roll downhill Bits of rock and soil may move
slowly, only a little at a time But at times they move very
quickly Heavy rains or earthquakes can loosen material that
is on a steep hill or slope Gravity then pulls this loose material
downward A landslide is the quick downhill movement of
great amounts of rock and soil Buildings, trees, and other large
objects may be swept down the slope with the sliding soil
8
Gravity and Avalanches
The rapid movement of objects down a slope can occur in cold areas as well An avalanche is fast-moving snow and ice that race down a mountain Strong winds, earthquakes, and explosions can cause avalanches People try to stop avalanches from happening They may clear snow before it builds up too much Landslides and avalanches can cause terrible damage, especially on large mountains
9
Trang 7Controlling Erosion and Deposition
Erosion and deposition often take place in areas with few
trees or plants Trees and plants help keep wind and water from
eroding rock and soil
People have found ways to slow the effects of erosion They
grow plants on the sides of hills Roots hold soil in place Plant
leaves keep some of the rain from washing soil away Farmers
whose fields are on a hill can plow them into steps, called
terraces Rain forms puddles on the steps instead of washing
soil downhill Crops can then soak up more water
11
Erosion can be a problem along the seashore as well Waves that pound against the shore carry away material, such as sand People build barriers to prevent this Barriers stop waves from eroding sand and rock Barriers also help protect nearby buildings and roads
People can reduce deposition They can dig away deposits from waterways This helps ships pass through the water more easily
Terraces slow the movement of water running downhill.
Trang 8How can Earth’s surface
change rapidly?
Volcanoes
A volcano is a
landform It can
cause a rapid
change to Earth’s
surface Hot rock,
called magma, has
partly melted into liquid
Gases push the magma up A
volcano forms at a weak spot in
Earth’s crust
A volcano erupts when magma boils onto
the surface Lava is magma that has come out of a
volcano Lava is still red hot
Pressure can build so much that the gases in the
magma explode Lava, gases, and ashes burst out
of openings called vents Not all volcanoes erupt
so wildly Magma oozes up and slowly flows out
of some volcanoes A bowl-shaped area, or crater,
may form around the volcano’s main opening
13
Effects of Eruptions
When volcanoes erupt, they form ash and new rock Ash from the eruption of Mount St Helens in 1980 flew more than
24 kilometers (15 miles) into the air It covered nearby cities It killed trees and animals
Active and Dormant Volcanoes
An active volcano erupts often or shows signs that it will erupt Kilauea in Hawaii began its latest eruption in 1983 It is still actively erupting
A dormant volcano has not erupted for a long time Mount Rainier in Washington has not had a big eruption in more than
500 years If it erupted, it could melt nearby glaciers This could cause flooding and landslides
An extinct volcano no longer erupts Mount Kenya in Africa
is one of many extinct volcanoes in the world
The 1980 eruption of Mount St Helens sent rock and ash into the air.
Trang 9Earth’s Moving Plates
Earth’s crust rests on a layer called the upper mantle
These layers form huge moving pieces called plates
The Cause of Earthquakes
A fault is a break or crack in rocks where Earth’s crust can
move Rocks may get stuck along a fault The plates keep
moving They press on the rocks that are stuck If the pressure
becomes strong enough, the rocks break The plates shift
quickly An earthquake is the sudden movement that makes
Earth’s crust shake
The focus is the underground spot where the plates shift and
the earthquake begins The epicenter is the point on Earth’s
surface above the focus The most damage is usually near the
epicenter Energy from an earthquake moves in waves
Epicenter Focus
Fault
15
Effects of Earthquakes and Volcanoes
Many places on Earth have earthquakes and volcanoes In
1815 Mount Tambora in Asia erupted Ash darkened the sky
Less sunlight reached Earth This caused snow to fall in the northeastern United States in June
In 1883 Krakatoa erupted in Indonesia This volcano caused huge waves called tsunamis in Earth’s oceans Earthquakes can also cause tsunamis Tsunamis can lead to landslides
Two plates meet in California along the San Andreas Fault
Many earthquakes happen along this fault Most are small
Some are very powerful
Weathering, erosion, and deposition change Earth’s landforms So do landslides, earthquakes, and volcanoes
Earth’s surface will always be changing
Earthquakes can cause great damage.
Trang 10Glossary
after erosion
Earth’s crust shake
where plates start to move
can move
surface
amounts of rock and soil
pours from below Earth’s crust
slowly break into smaller pieces
Vocabulary
deposition
earthquake
epicenter
erosion
fault
landform
landslide
volcano
weathering
What did you learn?
1 What can cause a landslide?
2 What makes magma rise inside a volcano?
3 Why do earthquakes happen at faults?
4 Erosion and deposition are two forces that change landforms Explain in your own words what each force does Include details from the book to support your answer.
weathering and chemical weathering alike? How are they different?
Illustration: 14 Alan Male
Photographs: Every effort has been made to secure permission and provide appropriate credit for
photographic material The publisher deeply regrets any omission and pledges to correct errors called to its
attention in subsequent editions Unless otherwise acknowledged, all photographs are the property of Scott
Foresman, a division of Pearson Education Photo locators denoted as follows: Top (T), Center (C), Bottom
(B), Left (L), Right (R) Background (Bkgd)
Opener: ©Hubert Stadler/Corbis; Title Page: ©Chris Reynolds and the BBC Team-Modlemakes/DK
Images; 4 ©AP/Wide World Photos; 5 ©Jack Dykinga/Getty Images; 7 (T) ©Richard Bickel/Corbis, (B)
©Owaki-Kulla/Corbis; 8 ©Paul A Souders/Corbis; 10 ©Dave G Houser/Corbis; 13 (TR, CR) ©Gary
Rosenquist; 15 ©George Hall/Corbis
ISBN: 0-328-13883-5
Copyright © Pearson Education, Inc
All Rights Reserved Printed in the United States of America This publication is
protected by Copyright and permission should be obtained from the publisher prior
to any prohibited reproduction, storage in a retrieval system, or transmission in any
form by any means, electronic, mechanical, photocopying, recording, or likewise For
information regarding permissions, write to: Permissions Department, Scott Foresman,
1900 East Lake Avenue, Glenview, Illinois 60025.
3 4 5 6 7 8 9 10 V010 13 12 11 10 09 08 07 06 05